Explaining a Soil Profile - senecahs.org
A soil profile is a vertical cross section of the soil. The differences are developed from the interaction of such soil-forming factors as parent material, slope, native vegetation, weathering, and climate. As a soil ages, horizontal layers develop and changes result. The causes of these
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Explaining a Soil Profile
www.senecahs.orgA soil profile is usually studied to a depth of 3 to 5 feet. To see the soil profile, soil cores may be taken or holes dug to expose the pro-file.
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www.senecahs.orgare responsible for most of the photosynthesis in the leaf and are called the palisade mesophyll. Located under the palisade mesophyll are loosely packed cells called the spongy mesophyll.
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www.senecahs.orgSoil Structure Sand, silt, clay, and organic-matter particles in a soil combine with one another to form larger particles of various shapes and sizes. These larger particles, or clusters, are often referred to as aggregates. The arrangement of the soil particles into aggregates of various sizes and shapes is soil structure.
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www.senecahs.orgAxillary bud Stipule Stem Petiole Blade FIGURE 1. The major parts of a leaf. Dicots have leaves with veins that connect and branch from each other. Veins in a branch-ing pattern are called netted veins. A leaf with netted veins sometimes has several smaller
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